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JJX-3019 Probe
PRODUCT PARAMETERS
- The structural design of the downhole instrument has been optimized, making the operation extremely simple, and the seismic performance of the instrument has been greatly improved, making it more durable.
- It integrates the functions of inclination measurement and natural gamma measurement, saving logging work time.
Description
JJX-3019 Borehole Deviation & Natural Gamma Probe
Abstract
JJX-3019 Borehole Deviation & Natural Gamma Probe is a digital logging tool that integrates natural gamma measurement and deviation measurement. The data measured downhole can be displayed in real time on the computer in the current measurement curve and chart. It also improves the natural gamma point measurement method that has been used to be continuous logging, which not only has high data collection efficiency, but also reduces the impact of human factors on the measurement data. It also has a large amount of information and high confidence, and will not miss abnormal sections.

Applicable Conditions
● Cased
● Bare hole fill with water or mud
● Bare Dry hole
Applications
● Coal, gas, nuclear, hydrology and other drilling guidance or drilling quality detection.
● Pile foundation engineering detection for water conservancy and hydropower, highway bridges, large buildings, etc.
● Estimation of uranium concentration.
● Dividing the stratum interface and judging the changes in the stratum phase.
Features
● The structural design of the downhole instrument has been optimized, making the operation extremely simple, and the seismic performance of the instrument has been greatly improved, making it more durable.
● It integrates the functions of inclination measurement and natural gamma measurement, saving logging work time.
Specifications
| Vertex angle measurement range | 0°~50°, Measurement accuracy: ±0.1°; Resolution: 0.01° |
| Azimuth measurement range | 0°~360° ,Measurement accuracy: ±2° (vertex angle 1°~15°) |
| Natural gamma measurement index | See the instruction manual of FD-3019 scintillation gamma logging tool |
| Measurement method | A) Point measurement according to depth; B) Continuous measurement according to depth |
| Signal output | Bipolar encoding |
FAQ
① In SI, it is m·s-2, and one percent of it is the international unit abbreviation g.u.;
② Conversion between SI and CGS: 1g.u.=10-1 mGal
Gravitational field: The space around the earth with gravity is called the gravitational field.
Gravitational potential: The gravitational potential W in the gravitational field is equal to the work done by a particle of unit mass moving from infinity to that point.
① The normal gravity field of the earth: Assuming that the earth is a rotating ellipsoid (reference plane), the surface is glossy, the internal density is uniform, or it is distributed in concentric layers, the density of each layer is uniform, and the deviation of the shape of the ellipsoid from the geoid is very small, then the gravity field generated by the earth is the normal gravity field.
② The normal gravity value is only related to the latitude, the smallest at the equator and the largest at the poles, with a difference of about 50,000 g.u.; the rate of change of the normal gravity value with latitude is the largest at 45° latitude, and zero at the equator and the poles; the normal gravity value decreases with increasing altitude, and its rate of change is -3.086 g.u.. The main feature of the long-term change is the "westward drift" of the geomagnetic elements, both the dipole field and the non-dipole field drift westward, and have a global nature.
The gravitational field strength is equal to the gravitational acceleration in both numerical and dimensional terms, and the two are in the same direction. In gravity exploration, all references to gravity refer to gravitational acceleration. The gravitational field strength at a point in space is equal to the gravitational acceleration at that point.
Gravity exploration is an exploration method that is based on the density difference of rocks and ores. Since density difference will cause local changes in the normal gravity field of the earth (i.e. gravity anomaly), it is used to solve geological problems by observing and studying gravity anomalies.
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